Biblio
Finite element modeling of ultrasound measurement systems for gas. Comparison with experiments in air. Journal of the Acoustical Society of America 144, (2018). Abstract
A model of solar coronal heating by classical inverse bremsstrahlung and generation of the solar wind. Astrophysical Journal 412, (1993).
Uncertainties in Arctic sea ice thickness and volume: new estimates and implications for trends. The Cryosphere 8, (2014).
Arctic Clouds and Surface Radiation – a critical comparison of satellite retrievals and the ERA-Interim reanalysis. Atmospheric Chemistry and Physics (ACP) 12, (2012).
Adaptively varying-coefficient spatiotemporal models. Journal of the Royal Statistical Society: Series B (Statistical Methodology) 71, (2009). Abstract
Total ozone variation between 50 and 60 N. Geophysical Research Letters 32, (2005). Last ned: 2005GL024012.pdf (225.86 KB)
Long-term variation in TOMS ozone over 60 deg.-70 deg. S. Geophysical Research Letters 24, 2295-2298 (1997).
On the exploitation of polarimetric ratio for oil spill detection. Electronic proceedings (EUSAR) 2016:7559371, (2016).
Modelling the ground layer (invited presentation). 2nd ARENA Workshop on Interferometry at Dome C. European Southern Observatory (ESO) and Max Planck Institute for Plasma Physics (IPP), Garching (Munich), Germany, October 13-14, 2008. Abstract: the web site of the EU FP6 project ARENA (2008).
Planetary boundary layer feedbacks in climate system and triggering global warming in the night, in winter and at high latitudes. Geography, Environment, Sustainability 1, (2009). Abstract
The nature and the role of semi-organised structures in the atmospheric convective boundary layers. Abstracts: 4th Annual Meeting of the European Meteorological Society, Nice, France, 26-30 September 2004 (2004).
On the velocity gradient in the stably stratified sheared flows. Part 1: Asymptotic analysis and applications. Boundary-Layer Meteorology 135, (2010). Abstract
Last ned: On the Velocity Gradient in Stably Stratified Sheared Flows. Part 2- Observations and Models.pdf (349.05 KB)
Atmospheric boundary layers in storms: advanced theory and modelling applications. The 6th Plinius International Conference on Mediterranean Storms (Genoa Naples Palermo Palma de Mallorca Barcelona Marseille Genoa), 17-24 October 2004. (2004).
The effect of large eddies on the convective heat/mass transfer over complex terrain: Advanced theory and its validation against experimental and LES data. Croatian Meteorological Journal 20-26 (2005).
Atmospheric planetary boundary layer feedback in climate system and triggering of climate change at high latitudes. EGU General Assembly 11, (2009).
The effect of stratification on the roughness length and displacement height. ICTP Fall Colloquium on the Physics of Weather and Climate: Regional Weather Predictability and Modelling, Trieste, Italy, 29 September 10 October 2008. Abstract: the Colloquium web site (2008).
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. Boundary-layer Meteorology 125, 167-191 (2007). Abstract
Last ned: fulltext-9.pdf (680.31 KB)
The Height of the Atmospheric Planetary Boundary layer: State of the Art and New Development. National Security and Human Health Implications of Climate Change (2012).doi:10.1007/978-94-007-2430-3_13
Atmospheric boundary layers in storms: advanced theory and modelling applications. Advances in Geosciences 47-49 (2005).
Similarity theory and calculation of turbulent fluxes at the surface for the stably stratified atmospheric boundary layer. Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security 37-49 (2007).på <http://www.springerlink.com.pva.uib.no/content/978-0-387-74318-9/#section=167162&page=3&locus=29> Abstract
Last ned: fulltext-10.pdf (911.87 KB)
The effect of stratification on the surface resistance for very rough vegetated and urban surfaces. Sixth International Conference on Urban Climate 415-418 (2006).
Resistance and heat transfer laws for stable and neutral boundary layers. Turbulence and Waves in Stably Stratified Atmospheric Shear Flows: Measurements, High Resolution Simulations and Numerical Prediction Challenges (2004).
Calculation of the height of stable boundary layers in practical applications. Boundary-layer Meteorology 389-409 (2002).på <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
